Statistical global and regional atmospheric models of temperature and gas components over the northern hemisphere

Numerical and the MU radar estimations of gravity wave enhancement and turbulent ozone fluxes near the tropopause

“…The estimates of Kdescribed above, together with the model of vertical ozone distribution (Zuev and Komarov, 1986), lead to the values of τ ∼0,3-3 days. These values show that the changes in IGW intensity and turbulence near the tropopause may lead, relatively fast, to the changes in the stratospheric ozone concentration and to a shift in the photochemical equilibrium.…”

“…Using the values of c for the altitudes of 12-17 km from the model of vertical ozone profile (Zuev and Komarov, 1986) and the values of K∼1-10 m 2 /s shown in Figs. 3 and 5, we may obtain the estimate F ∼(1-10)×10 14 m −2 s −1 .…”

Comparison between cross-track and conical scanning microwave window channels near 90 GHz

“…The 92-GHz Tb was calculated at <t > -1.5° and 40.5°, corresponding to the range of scanned nadirial angles for the variety of measured and simulated atmospheres encountered along the satellite ground track (representative oceanic profiles including eight climatological estimates [9]-[12], [22], 15 measurements from CEPEX and CASP experiments, and six coastal profiles from the NCDC sounding database [23] with SST's from the Oort database [11]). Calculations were repeated for M/I(<£ = 45°).…”

Web portal on environmental sciences &quot;ATMOS''

“…Here accessible are the model (Barker et al, 2003), the Frolkis model (Frolkis, 1993) as well as a software support for atmospheric transmittance function calculations (Kozodoeva and Firsov, 2005). The information part of the site contains data on two statistical models of atmosphere (Anderson, 1986;Zuev, 1986) and monograph by A. V. Vasiliev and I. N. Mel'nikova "Shortwave solar radiation in the Earth atmosphere: Calculations, measurements and interpretation". An example of a screenshot from the site is shown below.…”